The Amundsen Glacier is a major Antarctic glacier, about 7 to 11 km wide and 150 km (80 nmi) long. It originates on the Antarctic Plateau where it drains the area to the south and west of Nilsen Plateau, then descends through the Queen Maud Mountains to enter the Ross Ice Shelf just west of the MacDonald Nunataks.
Lillie Glacier is a large glacier in Antarctica, about 100 nautical miles long and 10 nautical miles wide. It lies between the Bowers Mountains on the west and the Concord Mountains and Anare Mountains on the east, flowing to Ob' Bay on the coast and forming the Lillie Glacier Tongue.
Tucker Glacier is a major valley glacier of Victoria Land, Antarctica, about 90 nautical miles long, flowing southeast between the Admiralty Mountains and the Victory Mountains to the Ross Sea. There is a snow saddle at the glacier's head, just west of Homerun Range, from which the Ebbe Glacier flows northwestward.
Mount Blackburn is the highest peak in the Wrangell Mountains of Alaska in the United States. It is the fifth-highest peak in the United States and the twelfth-highest peak in North America. The mountain is an old, eroded shield volcano, the second-highest volcano in the U.S. behind Mount Bona and the fifth-highest in North America. It was named in 1885 by Lt. Henry T. Allen of the U.S. Army after Joseph Clay Stiles Blackburn, a U.S. senator from Kentucky. It is located in the heart of Wrangell – St. Elias National Park, the largest national park in the country.
Triple Glaciers are in Grand Teton National Park, Wyoming, United States. The glaciers are disconnected from each other and occupy three separate cirques on the northwest face of Mount Moran and northeast of Thor Peak. The glaciers are unofficially referred to as East, Middle and West Triple Glacier.
The Dufek Massif is a rugged, largely snow-covered massif 27 nautical miles long, standing west of the Forrestal Range in the northern part of the Pensacola Mountains, Antarctica.
Rippon Glacier is a small glacier located in Kemp Land, East Antarctica. It is close east of Seaton Glacier, flowing southward into Edward VIII Ice Shelf.
The Batterbee Mountains are a group of prominent mountains rising to 2,200 metres (7,200 ft), which forms part of the dissected edge of Dyer Plateau overlooking George VI Sound, on the west coast of Palmer Land. First seen and photographed from the air by Lincoln Ellsworth on 23 November 1935, they were charted from the ground in October 1936 by the British Graham Land Expedition (BGLE) under John Rymill, and named after Sir Harry Batterbee (1880–1976), Assistant Under-Secretary of State, Dominions Office, 1930–38, and Chairman of the Polar Committee in 1934, who gave help to the expedition.
The Butler Glacier is a broad glacier draining the north side of Edward VII Peninsula in the vicinity of Clark Peak, and flowing generally northeastward through the Alexandra Mountains to its terminus in Sulzberger Bay.
Mount Jumper is a mountain 2,890 metres (9,480 ft) high located 7 nautical miles (13 km) east of Mount Viets in the central part of the Sentinel Range of the Ellsworth Mountains in Antarctica. Debren Pass separates it from the side ridge descending via Evans Peak. The mountain overlooks Ellen Glacier to the north and east, and its tributaries Patton Glacier and Rumyana Glacier to the south and northwest respectively.
Rampart Ridge is a prominent broken ridge on the west side of the Royal Society Range, Antarctica. It stands north of Rutgers Glacier and extends from The Spire to Bishop Peak.
Inspiration Glacier is on the east slopes of Eldorado Peak, North Cascades National Park in the U.S. state of Washington. The glacier is approximately 1.5 mi (2.4 km) in length, 2 mi (3.2 km) in width at its terminus and descends from 8,500 to 6,800 ft. Inspiration Glacier lies in a cirque with Eldorado Peak to the west, the arête known as Tepeh Towers to the northwest and Klawatti Peak to the northeast. Inspiration Glacier is connected to the Eldorado Glacier to the south and partially separated by the Tepeh Towers from the McAllister Glacier to the north. Meltwaters from Inspiration Glacier flow into Moraine Lake.
Klawatti Glacier is located on the east slopes of Klawatti Peak, North Cascades National Park, in the U.S. state of Washington. The glacier is approximately .85 mi (1.37 km) in length, 1.2 mi (1.9 km) in width at its terminus and descends from 8,000 to 6,600 ft, where it terminates above Klawatti Lake. Arêtes separate Klawatti Glacier from Inspiration Glacier to the southwest, McAllister Glacier to the northwest and North Klawatti Glacier to the north.
Spire Glacier is in Snoqualmie National Forest in the U.S. state of Washington and is on the west slopes of Spire Point. Spire Glacier flows generally northwest for a distance of approximately .50 mi (0.80 km). An arête separates the glacier from Dana Glacier to the east. Spire Glacier descends from nearly 7,400 to 6,000 ft.
Dome Glacier is in Snoqualmie National Forest in the U.S. state of Washington and is on the north slopes of Dome Peak. Dome Glacier flows generally west for a distance of approximately .80 mi (1.29 km), maintaining a generally shallow gradient between 8,600 to 7,600 ft at which point it descends in a large icefall to approximately 6,900 ft (2,100 m). An arête separates the glacier from Dana Glacier to the northwest and Chickamin Glacier to the east.
Neve Glacier is in North Cascades National Park in the U.S. state of Washington and is on the north slopes of Snowfield Peak. Neve Glacier flows generally north and splits in two with two terminal tongues, one flowing to the northwest which is known as Ladder Creek Glacier and the other descending a total of more than 1.8 mi (2.9 km) to the east. Ladder Creek Glacier descends from 7,800 to 6,000 ft, while the east tongue also originates from the same altitude and descends to 5,600 ft (1,700 m). Between 1850 and 2006, Neve Glacier is estimated to have retreated more than 1,000 m (3,300 ft).
Pilz Glacier is in Wenatchee National Forest in the U.S. state of Washington and is on the north slopes Luahna Peak. Pilz Glacier descends from 8,000 to 6,900 ft. An arête separates Pilz Glacier from Butterfly Glacier to the west. Pilz Glacier is within the Glacier Peak Wilderness and is just over 6.5 mi (10.5 km) southeast of Glacier Peak.
Noisy Creek Glacier is in North Cascades National Park in the U.S. state of Washington, .50-mile (0.80 km) northwest of Bacon Peak. Noisy Creek Glacier has retreated and left behind a series of small proglacial lakes. Noisy Creek Glacier descends from 6,300 to 5,500 ft and had an area of .58 km2 in 1993. A ridge separates Noisy Creek Glacier from Green Lake Glacier to the east. The National Park Service is currently studying Noisy Creek Glacier as part of their glacier monitoring project. Between 1993, and 2013 the glacier had lost ~8 m of thickness.
Hinkley Glacier is a glacier flowing northeastward from Corbet Peak and Schoening Peak, Vinson Massif on the east slope of Sentinel Range in the Ellsworth Mountains, Antarctica, and continuing between Mount Segers and Zinsmeister Ridge to enter Dater Glacier southeast of Nebeska Peak and northwest of Sipey Bluff. It was named by US-ACAN (2006) after Todd K. Hinkley, Technical Director, National Ice Core Laboratory, U.S. Geological Survey, Denver, CO,2001-06.
